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Mystic Creek Member

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Journal Article
Journal: Economic Geology
Published: 01 November 2012
Economic Geology (2012) 107 (7): 1403–1432.
..., and interlayered pyritic argillite and mudstone of the Mystic Creek Member of the Totatlanika Schist Formation. Mystic Creek metarhyolite and alkali basalt (Chute Creek Member) constitute a bimodal pair that formed in an extensional environment. A synvolcanic peralkaline quartz porphyry containing veins...
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Journal Article
Published: 01 August 2007
Geochemistry: Exploration, Environment, Analysis (2007) 7 (3): 207–223.
... rocks of the Mystic Creek Member of the Totatlanika Schist. Water samples with the lowest pH (many below 3.5), highest specific conductance (commonly >2500 μS/cm) and highest major- and trace-element concentrations are from springs and streams within the quartz–sericite–pyrite alteration zone...
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Image
Rare earth element patterns for filtered/acidified waters within the altera...
Published: 01 August 2007
Fig. 13 Rare earth element patterns for filtered/acidified waters within the alteration zone at Red Mountain and surrounding unmineralized felsic metavolcanic rocks of the Mystic Creek Member, normalized to North American Shale Composite.
Image
Regional and detailed geological maps of the Red Mountain deposit and vicin...
Published: 01 August 2007
in Grayd Resources Corporation 1998 ). All rock units in (b) are part of the Mystic Creek Member of the Totatlanika Schist.
Image
Distribution of Zn in stream sediment samples. The local background value i...
Published: 01 August 2007
Fig. 9 Distribution of Zn in stream sediment samples. The local background value is an average from 25 unmineralized rock samples collected from the Mystic Creek Member of the Totatlanika Schist ( Dusel-Bacon et al . 2004 ; C. Dusel-Bacon, unpubl. data). White line indicates the approximate
Image
Geologic map of the Wood River area (after  Wahrhaftig, 1968 ,  1970 ;  Gil...
Published: 01 November 2012
the locations of whole-rock geochemical samples from the western area of the Mystic Creek Member presented in Table 1 , columns H, I, and J, respectively.
Image
SEM photomicrographs of Ce-La-F-O accessory minerals in polished thin secti...
Published: 01 August 2007
Fig. 14 SEM photomicrographs of Ce-La-F-O accessory minerals in polished thin sections of Mystic Creek Member metarhyolite from the Red Mountain area. (a) Secondary electron image of drill core sample DC-96-3A-273. (b) Backscattered electron image of rock sample 97ADb60G in which inclusions
Image
Elemental plots of whole-rock data for mineralized and unmineralized argill...
Published: 01 November 2012
felsic metaigneous rocks from the Bonnifield district ( Dusel-Bacon et al., 2004 , 2010 ): dotted line = peralkaline metarhyolite from the Mystic Creek Member of the Totatlanika Schist; dash-dot line = felsic rocks from the Sheep, California, and Moose Creek Members of the Totatlanika Schist; dashed
Image
Field, surface sample, and drill core photos from the Bonnifield deposits. ...
Published: 01 November 2012
, plagioclase, and K-feldspar in a fine-grained quartzofeldspathic and sericitic matrix (DC North zone). C. N-dipping sequence of mostly Mystic Creek Member metavolcanic rocks south of Red Mountain; upper arrow points to peralkaline metarhyolite plug and lower arrow points to a >10-m-thick layer
Journal Article
Journal: GSA Bulletin
Published: 01 July 2004
GSA Bulletin (2004) 116 (7-8): 989–1015.
... northeast of the Salcha River gneiss dome, in a topographically high area that includes rugged West Point peak (Fig. 4) . Prior to our U-Pb dating of these rocks, the only age control consisted of conodonts of Middle Devonian to Early Mississippian age at one location within the Mystic Creek Member...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 October 2014
Lithosphere (2014) 6 (5): 383–398.
... in these localities are thought to roughly overlap in age with Mississippian–Permian units in the Mystic Pass and Farewell Lake–Sheep Creek localities, exposures are sparse and very limited. This study focuses on Mississippian–Permian stratigraphy exposed in the northwestern Talkeetna quadrangle (Mystic Pass region...
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Journal Article
Journal: Geosphere
Published: 30 May 2018
Geosphere (2018) 14 (4): 1501–1543.
... that of the fossiliferous sandstone. It has some statistical similarity to samples 11AD2A (Sheep Creek Formation; Fig. 7A ) and 03ADw415C (lower Mystic assemblage; Fig. 8A ), producing PDP cross-correlation coefficients of 0.51 and 0.58, respectively (Table S3 [ footnote 1 ]; Saylor and Sundell, 2016 ). Otherwise...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1941
AAPG Bulletin (1941) 25 (1): 23–72.
... for the three limestone members of the Fort Scott formation and he (letter dated, January 5, 1940) has kindly consented. Greene proposes to substitute the name Blackjack Creek limestone for lower Fort Scott. For a type locality he refers to outcrops in Johnson County mentioned by Hinds (1912, p. 220); “Four...
FIGURES
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 11 October 2017
Lithosphere (2017) 9 (6): 927–952.
... (augen orthogneiss in the California Creek Member of the Totatlanika Schist) and 367 ± 4 Ma to 356 ± 3 Ma (metarhyolite in the Moose Creek and Mystic Creek Members of the Totatlanika Schist) ( Dusel-Bacon et al., 2004 , 2012 ). Most of the metarhyolite in the Mystic Creek Member is interpreted...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1975
AAPG Bulletin (1975) 59 (7): 1126–1135.
... and argillaceous dolomites which range in thickness from 20 to 45 ft, is conformable on the Connell Sandstone Member but unconformable beneath the massive carbonate rocks of the Montoya Group. In subsurface, the carbonate rocks of the Oil Creek Formation underlie the Waddell Sandstone Member of the McLish...
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Journal Article
Published: 01 June 2013
Bulletin of the Seismological Society of America (2013) 103 (3): 2047–2061.
... the likelihood of a rupture jumping across the stepover. Our new cone penetration test ( CPT ) and trench observations along the Claremont fault at Mystic Lake indicate that the main strand of the Claremont fault has jumped nearly a half kilometer westward into the San Jacinto releasing stepover during the late...
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Journal Article
Published: 01 March 2019
Journal of Paleontology (2019) 93 (2): 244–259.
... bottom to top are the Bull Creek Member, Bee Cave Member, Cedar Park Member, Whitestone Member, Keys Valley Member, and an unnamed “upper marl member.” The Bull Creek Member is made up of hard, burrowed, nodular limestone. In the western Austin area of Travis County, the Bull Creek Member varies...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1942
AAPG Bulletin (1942) 26 (10): 1585–1593.
... the limestone closely overlies the very pimply, black, sheety roof shale of the coal which also in both states locally rises considerably above the coal, because of the presence of the lenticular Francis Creek shale. Other members of the Oak Grove succession have not been certainly recognized in Iowa...
FIGURES
Journal Article
Journal: Geosphere
Published: 26 February 2018
Geosphere (2018) 14 (2): 367–394.
... lithologic and faunal features that suggest ties to the Farewell terrane ( Blodgett et al., 2002 ; Dumoulin et al., 2014a ). Lower Paleozoic rocks in the White Mountains terrane comprise a mafic volcanic succession (Ordovician Fossil Creek Volcanics) overlain by shallow-water carbonate strata (Silurian...
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Journal Article
Published: 30 January 2012
Canadian Journal of Earth Sciences (2012) 49 (1): 59–90.
... of the Cow Head Group and Lower Head Formation. James and Stevens (1986) mapped the whole group in great detail and formally established two formations and seven members ( Fig. 3 ). The two formations reflect both the nature and depositional setting of the Cow Head Group sediments. The Shallow Bay...
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